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1.
Figure 2

Figure 2. Winter Snow Depths 1948–2003 at Tower Falls. From: Gray Wolves as Climate Change Buffers in Yellowstone.

Average monthly SDTH for November (A), December (B), January (C), February (D), March (E), and April (F) 1948–2003 at the Tower Falls weather site.

Christopher C Wilmers, et al. PLoS Biol. 2005 Apr;3(4):e92.
2.
Figure 1

Figure 1. Winter Snow Depths 1948–2003 at Mammoth Hot Springs. From: Gray Wolves as Climate Change Buffers in Yellowstone.

Average monthly SDTH for November (A), December (B), January (C), February (D), March (E), and April (F) 1948–2003 at the Mammoth Hot Springs weather site.

Christopher C Wilmers, et al. PLoS Biol. 2005 Apr;3(4):e92.
3.
Figure 5

Figure 5. Change in Carrion Available to Scavengers due to Climate Change 1950–2000: Dynamic Model. From: Gray Wolves as Climate Change Buffers in Yellowstone.

Shown is the mean monthly change (± standard error) in carrion available to scavengers due to climate change from 1950 to 2000 with and without wolves in our dynamic model.

Christopher C Wilmers, et al. PLoS Biol. 2005 Apr;3(4):e92.
4.
Figure 4

Figure 4. Reduction in Winter Carrion Available to Scavengers due to Climate Change 1950–2000: Statistical Model. From: Gray Wolves as Climate Change Buffers in Yellowstone.

Shown are percent reductions (± standard error) in winter carrion available to scavengers due to climate change from 1950 to 2000 with and without wolves in our statistical model. * Significant difference between the two scenarios.

Christopher C Wilmers, et al. PLoS Biol. 2005 Apr;3(4):e92.
5.
Figure 3

Figure 3. Changes in the Last Day of Snow Cover over the Last 55 Years at Mammoth Hot Springs and Tower Falls. From: Gray Wolves as Climate Change Buffers in Yellowstone.

Last day of snow cover is reported as the number of days from January 1 of that year until the first day of bare ground. Changes in last day of snow cover over the last 55 y are shown for Mammoth Hot Springs (A) and Tower falls (B). The number of days from January through March that temperatures exceeded freezing at Mammoth (C) and Tower (D) are increasing with time.

Christopher C Wilmers, et al. PLoS Biol. 2005 Apr;3(4):e92.

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